“…The first step is the initial acceleration of bulk ion upflow events driven by ion heating and ambipolar diffusion as observed by incoherent scatter radars (ISRs) [ Wahlund et al ., ; Ogawa et al ., , , ; Buchert et al ., ; Skjæveland et al ., ], sounding rockets [ Arnoldy et al ., ; Lynch et al ., ; Frederick‐Frost et al ., ], and satellites in polar low Earth orbit in the F region ionosphere [ Coley et al ., ; Ogawa et al ., ; Lühr et al ., ; Chaston et al ., ; Lorentzen et al ., ; Sadler et al ., ]. The second step is that upflow events that have reached sufficiently high altitudes are exposed to wave energies available in the topside ionosphere/magnetosphere which drive nonthermal transverse acceleration of oxygen [ André and Yau , ; Strangeway et al ., ; Chaston et al ., ; Jacobsen and Moen , ].…”